This Pallasite Meteorite has been displayed in a museum quality deep box frame. This specimen is a rare stony-iron meteorite dating back approximately 4.5 billion years.
Composed of nickel-iron metal embedded with transparent olivine crystals, this meteorite represents the boundary between the core and mantle of a differentiated asteroid. The olivine inclusions, often referred to as peridot when gem-quality, are naturally encased within the metallic matrix, creating a unique and striking texture.
Recovered from a recognised fall site, the specimen preserves the complex interplay of metal and mineral that formed deep within an ancient planetary body.
The picture shown is an example of the quality that you can expect to receive. Please be aware that, as these are natural products, they are subject to some variation.
